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基于SPI/SPEI的黑龙江省干旱特征对比分析OA

Comparative Analysis of Drought Characteristics in Heilongjiang Province Based on SPI/SPEI

中文摘要英文摘要

为筛选黑龙江省干旱监测的最优指标方案,更好地应对气象变化,制定精细化抗旱策略,基于黑龙江省30个站点逐日气象数据资料计算不同尺度的SPI和SPEI,对比分析两种指数在干旱趋势识别与空间分布特征上的差异.结果表明,黑龙江省1971-2020年整体呈显著湿润化趋势且季节差异明显,春季、冬季均呈显著湿润化趋势,夏季、秋季呈不显著湿润化趋势.两种指数趋势一致性较高,但SPEI受蒸散影响,波动幅度强于SPI;SPI与SPEI的识别敏感性存在差异:春季SPI反映的干旱程度更强,夏秋冬季节SPEI更能捕捉干旱强度;特旱、轻旱SPI识别更全面,重旱SPEI更敏感,中旱两种指数识别结果较为一致;干旱在空间分布上呈现出明显的区域差异,且受地形因素的调控作用显著.重旱高频区集中于东南部,SPEI识别的重旱频率呈东高西低分布,且平原区显著高于山地区,SPI识别的重旱分布更均匀、强度更弱;特旱高频区位于西北部,山地区特旱频率显著高于平原区,SPI识别的特旱分布更广,SPEI识别的特旱频率整体偏低;总体上,SPI识别的黑龙江省总干旱频次略高于SPEI.

In order to determine the optimal indicator system for drought monitoring in Heilongjiang Province,adapt to meteorological variations more effectively and develop refined drought mitigation strategies.Based on daily meteorological data from 30 stations in Heilongjiang Province,the Standardized Precipitation Index(SPI)and Standardized Precipitation Evapotranspiration Index(SPEI)at different time scales were calculated to compare and analyze the differences between the two indices in drought trend identification and spatial distribution characteristics.The results showed that,Heilongjiang Province exhibited a significant overall wetting trend from 1971 to 2020 with obvious seasonal variations-significant wetting trends were observed in spring and winter,while non-significant wetting trends occurred in summer and autumn.The two indices showed high consistency in trend,but SPEI,affected by evapotranspiration,had a greater fluctuation amplitude than SPI.There were differences in identification sensitivity between SPI and SPEI,SPI reflected more severe droughts in spring,while SPEI was more effective in capturing drought intensity in summer,autumn,and winter.SPI identified extreme droughts and mild droughts more comprehensively,SPEI was more sensitive to severe droughts,and the two indices showed consistent results in identifying moderate droughts.Drought exhibited obvious regional differences in spatial distribution,with significant regulation by topographic factors.High-frequency areas of severe drought were concentrated in the southeastern part,SPEI indicated that the frequency of severe drought was higher in the east than in the west,and significantly higher in plain areas than in mountainous areas,while SPI showed a more uniform distribution of severe drought with weaker intensity.High-frequency areas of extreme drought were located in the northwestern part,where the frequency was significantly higher in mountainous areas than in plain areas,SPI identified a wider distribution of extreme drought,while SPEI generally indicated a lower frequency of extreme drought.Overall,the total drought frequency in Heilongjiang Province identified by SPI was slightly higher than that by SPEI.

刘佳丽;杜崇

黑龙江大学水利电力学院,黑龙江哈尔滨 150080黑龙江大学水利电力学院,黑龙江哈尔滨 150080

SPISPEI黑龙江省干旱时间尺度空间分布

Standardized Precipitation IndexStandardized Precipitation Evapotranspiration IndexHeilongjiang Provincedroughttemporal scalespatial distribution

《黑龙江农业科学》 2026 (3)

22-32,11

黑龙江省自然科学基金项目(LH2023E109).

10.11942/j.issn1002-2767.2026.03.0022

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